How wide is a road? The association of roads and mass-wasting in a forested montane environment

A spatial data base of 1609 landslides was analysed using a geographic information system to determine landslide frequency in relation to highways. A 126 km long transportation network in a 201km 2 area of humid-tropical, mountainous, forested terrain in Puerto Rico was used in conjunction with a series of 20 buffer (disturbance) zones varying from 5 to 400 m in length, measured perpendicular to the highways. Average landslide frequency in the study area at distances greater than 85 m from roads was about six landslides per square kilometre. At distances of 85 m or less on either side of a highway, landslide frequency was about 30 landslides per square kilometre. On average, this elevated disturbance rate affected 330 m 2 km -2 a -1 within the 170 m swath. The mass-wasting rate outside of the disturbance zone affected 40 m 2 km -2 a -1 . These results indicate that the rate of mass-wasting disturbance is increased from five to eight times in a 170 m wide swath along road corridors. The lateral extent of the environmental impact of roads in the study area is greater than is commonly perceived. The approach described herein demonstrates a simple method to assess the spatial association of mass-wasting with highways. © 1997 by John Wiley & Sons, Ltd.

[1]  Martin Haigh,et al.  Environmental correlations of landslide frequency along new highways in the Himalaya: Preliminary results , 1988 .

[2]  Road-cut slope topography and stability relationships in St Lucia, West Indies , 1983 .

[3]  Andrew Simon,et al.  Rainfall-threshold conditions for landslides in a humid-tropical system , 1993 .

[4]  R. Beschta Long-Term Patterns of Sediment Production Following Road Construction and Logging in the Oregon Coast Range , 1978 .

[5]  P. Reichenbach,et al.  GIS techniques and statistical models in evaluating landslide hazard , 1991 .

[6]  R L Shuster,et al.  Landslides: Analysis and Control , 1978 .

[7]  A. J. Sánchez,et al.  Landslides Triggered by Hurricane Hugo in Eastern Puerto Rico , September 1989 , 1997 .

[8]  E. Brabb The San Mateo County California Gis Project for Predicting the Consequences of Hazardous Geologic Processes , 1995 .

[9]  Frederick N. Scatena,et al.  The effect of human activity on the structure and composition of a tropical forest in Puerto Rico , 1994 .

[10]  R. Sidle,et al.  Hillslope stability and land use , 1985 .

[11]  T. Donnelly Geologic history of the Caribbean and Central America , 1989 .

[12]  John W. Williams,et al.  Rates of Landsliding as Impacted by Timber Management Activities in Northwestern California , 1986 .

[13]  Sediment discharge from an area of highway construction, Applemans Run basin, Columbia County, Pennsylvania , 1976 .

[14]  Andrew Simon,et al.  A rainfall intensity-duration threshold for landslides in a humid- tropical environment, Puerto Rico , 1993 .

[15]  Frederick N. Scatena,et al.  Physical aspects of Hurricane Hugo in Puerto Rico , 1991 .

[16]  R. Maharaj Landslide processes and landslide susceptibility analysis from an upland watershed: A case study from St. Andrew, Jamaica, West Indies , 1993 .

[17]  M. Larsen,et al.  Geographic relations of landslide distribution and assessment of landslide hazards in the Blanco, Cibuco, and Coamo basins, Puerto Rico , 1996 .

[18]  W. McDowell,et al.  Export of carbon, nitrogen, and major ions from three tropical montane watersheds , 1994 .

[19]  D. Varnes SLOPE MOVEMENT TYPES AND PROCESSES , 1978 .

[20]  Andrew C. Millington,et al.  Humid Tropical Environments. , 1995 .

[21]  R. Birdsey,et al.  Forest Area Trends in Puerto Rico , 1987 .